机译:伊朗东部锡斯坦缝合线地区的白垩纪高压变质作用和低压套印:榴辉岩的额外温度估算,U-Pb锆石年龄的地质意义以及Rb-Sr限制在发掘时间上
Westfal Wilhelms Univ Munster, Inst Mineral, Corrensstr 24, D-48149 Munster, Germany|Eberhard Karls Univ Tubingen, Isotopengeochem, Wilhelmstr 56, D-72074 Tubingen, Germany;
Westfal Wilhelms Univ Munster, Inst Mineral, Corrensstr 24, D-48149 Munster, Germany;
Univ Birjand, Dept Min Engn, Birjand, Iran;
Westfal Wilhelms Univ Munster, Inst Mineral, Corrensstr 24, D-48149 Munster, Germany;
Univ Bremen, FB Geowissensch 5, PF 330 440, D-28334 Bremen, Germany;
Rb-Sr geochronology; Ti-in-zircon; Zr-in-rutile; Sistan ocean; Neotethys; Iran;
机译:高压变质的时间和榴辉岩类型局部的发掘(Kupplerbrunn-Prickler Halt,Saualpe,奥地利东南部):Sm-Nd,Lu-Hf,U-Pb和Rb-Sr同位素系统相关性的限制
机译:伊朗东部锡斯坦缝合带高压变质岩的早白垩世掘出
机译:加拿大山脉Yukon-Tanana地层高压变质的时间:来自Teslin构造带的榴辉岩U-Pb锆石年代的约束